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2011年台风"南玛都"不同阶段降水结构特征

钟文婷 白爱娟 蔡亲波

热带地理2015,Vol.35Issue(3):334-342,9.
热带地理2015,Vol.35Issue(3):334-342,9.

2011年台风"南玛都"不同阶段降水结构特征

Precipitation Structural Characteristics in Different Stages of Typhoon'Nanmadol'in 2011

钟文婷 1白爱娟 2蔡亲波1

作者信息

  • 1. 成都信息工程学院 大气科学学院,成都 610225
  • 2. 海南省海口市气象局,海口 571100
  • 折叠

摘要

Abstract

Based on the TRMM satellite data and NCAR/NCEP reanalysis data, this paper analyses the variations of precipitation characteristics of Typhoon'Nanmadol'in 2011, especially its thermal and dynamic structures in its weakening phase after landing on the south part of Taiwan Island. The results show that: 1) The rainfall distribution of 'Nanmadol' is significantly asymmetric, and severe precipitation occurs at the eye-wall region, which mainly resulted from the convective cloud, but stratiform cloud contributes much to the total rainfall of typhoon than convective clouds. Within the four kinds of particles in the clouds, the content of cloud-water particles is the lowest, followed by ice-water, and the content of rain-water particles is the most than any others. Around the typhoon, precipitation mainly occurs in its southwest direction during the stage of infancy and weakening, but in the southeast direction in maturity stage with a more clear and complete structure. 2) The precipitation cloud of'Nanmadol'is columnar in the vertical direction and can be extended up to about 10 km, while the heavy rainfall echo concentrates below the height of 5 km, especially at the level of 2-4km. 3) After its landing, severe precipitation mainly occurs in its southwest direction, but in other orientations there is scattered and weak rainfall. The warm-moist core of typhoon inclines towards southwest with the height. At the same time the strong latent heat releases at the middle troposphere, which is about the height of 5km. In one word, the air flows in the typhoon from the lower troposphere with strong convergence, and flows out it at the level of the tropopause with divergence in the unstable atmospheric stratification, which is benefit to the formation of heavy rainfall in the southwest part of typhoon center.

关键词

TRMM卫星/"南玛都"台风/降水结构

Key words

TRMM Satellite/Typhoon'Nanmadol'/precipitation structure

分类

天文与地球科学

引用本文复制引用

钟文婷,白爱娟,蔡亲波..2011年台风"南玛都"不同阶段降水结构特征[J].热带地理,2015,35(3):334-342,9.

基金项目

国家科技支撑项目(2013BAK05B00) (2013BAK05B00)

热带地理

OACSTPCD

1001-5221

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